Excess 234U: An aging effect in confined waters

J. Kronfeld*, E. Gradsztajn, H. W. Müller, J. Radin, A. Yaniv, R. Zach

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

Abstract

Strong isotopic fractionation between 234U and 238U has been noted in deep oil-well brines. The waters are stratigraphically and structurally isolated from fresh-water inflow and have remained stagnant for more than five half-lifes of 234U. Excess 234U is explained by the 234Th alpha-recoil nucleus event.

Original languageEnglish
Pages (from-to)342-345
Number of pages4
JournalEarth and Planetary Science Letters
Volume27
Issue number2
DOIs
StatePublished - Sep 1975

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